Relevant bibliographies by topics / Chandra basin

Academic literature on the topic 'Chandra basin'

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Published: 6 September 2023

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Journal articles on the topic "Chandra basin"

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Kulkarni, Anil V., Sunil Dhar, B. P. Rathore, Babu Govindha Raj K., and Rajeev Kalia. "Recession of samudra tapu glacier, chandra river basin, Himachal Pradesh." Journal of the Indian Society of Remote Sensing 34, no. 1 (March 2006): 39–46. http://dx.doi.org/10.1007/bf02990745.

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Pandey, Pratima, S. Nawaz Ali, AL Ramanathan, P. K. Champati ray, and G. Venkataraman. "Regional representation of glaciers in Chandra Basin region, western Himalaya, India." Geoscience Frontiers 8, no. 4 (July 2017): 841–50. http://dx.doi.org/10.1016/j.gsf.2016.06.006.

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Dutta, Shruti, and AL Ramanathan. "Estimation of Deglaciation through Remote Sensing Techniques in Chandra-Bhaga Basin, Western Himalaya." Journal of Climate Change 7, no. 1 (February 3, 2021): 79–88. http://dx.doi.org/10.3233/jcc210007.

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Glaciers act as natural indicators of climate response and natural buffers of the hydrological cycle. Hence, continuous monitoring of glaciers is very crucial for which remote sensing techniques have emerged as a powerful tool to understand the micro-level variation and dynamics of glaciers. Unfortunately, a database involving complete basin-level approach and an extensive temporal range is not available for the entire Chandra-Bhaga (CB) sub-basin. Thus, the present investigation attempts to account for the extent of deglaciation in the CB basin showing that 16.7 percent of the glaciated area has been lost during 1989-2019. Moreover, the last three decades have witnessed a rapid rate of loss for small and medium-sized glaciers as compared to larger glaciers. Adding to it, the basin has also shown an upwards shift of mean elevation in this period. Over the last decade, an increasing temperature in the western Himalayas and Hindu Kush regions, as asserted by previous studies, have led to spatio-temporal changes in the glaciated area. The extent of deglaciation alongwith the glacier-climate behaviour and response can also provide a link to measure the topographical parameters.
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Majeed, Zahid, Muneer Ahmad Mukhtar, Riyaz Ahmad Mir, Pawan Kumar, and Kalyan Krishna. "Sonapani Glacier Recession over a Century from 1906–2016, Chandra Basin, Himachal Himalaya." Journal of the Geological Society of India 95, no. 1 (January 2020): 36–44. http://dx.doi.org/10.1007/s12594-020-1384-5.

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Sahu, Rakesh, and R. D. Gupta. "Glacier mapping and change analysis in Chandra basin, Western Himalaya, India during 1971–2016." International Journal of Remote Sensing 41, no. 18 (June 30, 2020): 6914–45. http://dx.doi.org/10.1080/01431161.2020.1752412.

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Prakash, Chander, and R. Nagarajan. "Glacial lake changes and outburst flood hazard in Chandra basin, North-Western Indian Himalaya." Geomatics, Natural Hazards and Risk 9, no. 1 (January 1, 2018): 337–55. http://dx.doi.org/10.1080/19475705.2018.1445663.

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Pandit, Ankur, and RAAJ Ramsankaran. "Modeling ice thickness distribution and storage volume of glaciers in Chandra Basin, western Himalayas." Journal of Mountain Science 17, no. 8 (July 17, 2020): 2011–22. http://dx.doi.org/10.1007/s11629-019-5718-y.

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Tawde, Sayli Atul, Anil V. Kulkarni, and Govindasamy Bala. "An estimate of glacier mass balance for the Chandra basin, western Himalaya, for the period 1984–2012." Annals of Glaciology 58, no. 75pt2 (July 2017): 99–109. http://dx.doi.org/10.1017/aog.2017.18.

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ABSTRACTAn improved understanding of fresh water stored in the Himalaya is crucial for water resource management in South Asia and can be inferred from glacier mass-balance estimates. However, field investigations in the rugged Himalaya are limited to a few individual glaciers and short duration. Therefore, we have recently developed an approach that combines satellite-derived snowlines, a temperature-index melt model and the accumulation-area ratio method to estimate annual mass balance of glaciers at basin scale and for a long period. In this investigation, the mass balance of 146 glaciers in the Chandra basin, western Himalaya, is estimated from 1984 to 2012. We estimate the trend in equilibrium line altitude of the basin as +113 m decade−1and the mean mass balance as −0.61 ± 0.46 m w.e. a−1. Our basin-wide mass-balance estimates are in agreement with the geodetic method during 1999–2012. Sensitivity analysis suggests that a 20% increase in precipitation can offset changes in mass balance for a 1 °C temperature rise. A water loss of 18% of the total basin volume is estimated, and 67% for small and low-altitude glaciers during 1984–2012, indicating a looming water scarcity crisis for villages in this valley.
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Rastogi, G., and Ajai. "Comparison of energy balance on Gangotri and Chhota Shigri Glaciers." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XL-8 (November 28, 2014): 537–42. http://dx.doi.org/10.5194/isprsarchives-xl-8-537-2014.

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Surface energy balance of a glacier governs the physical processes taking place at the surface-atmosphere interface and connects ice ablation/accumulation to climate variability. To understand the response of Himalayan glaciers to climatic variability, a study was taken to formulate energy balance equation on two of the Indian Himalayan glaciers, one each from Indus and Ganga basins, which have different climatic and physiographic conditions. Study was carried out over Gangotri glacier (Ganga basin) and Chhota Shigri(CS) glacier from Chandra sub-basin (Indus basin). Gangotri glacier is one of the largest glaciers in the central Himalaya located in Uttarkashi District, Uttarakhand, India. Chhota Shigri glacier of Chandra sub-basin lies in Lahaul and Spiti valley of Himachal Pradesh. Energy balance components have been computed using inputs derived from satellite data, AWS (Automatic Weather Station) data and field measurements. Different components of energy balance computed are net radiation (includes net shortwave and net longwave radiation), sensible heat flux and latent heat flux. In this study comparison has been made for each of the above energy balance components as well as total energy for the above glaciers for the months of November and December, 2011. It is observed that net radiation in Gangotri glacier is higher by approximately 43 % in comparison to Chhota Shigri glacier; Sensible heat flux is lesser by 77 %; Latent heat flux is higher by 66 % in the month of November 2011. Comparison in the month of December shows that net radiation in Gangotri glacier is higher by approximately 22 % from Chhota Shigri glacier; Sensible heat flux is lesser by 90 %; Latent heat flux is higher by 3 %.Total energy received at the glacier surface and contributes for melting is estimated to be around 32 % higher in Gangotri than Chhota Shigri glacier in November, 2011 and 1.25 % higher in December, 2011. The overall results contribute towards higher melting rate in November and December, 2011 in Gangotri than Chhota Shigri glacier.
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Pandey, Aayushi, Aman Rai, Sharad Kumar Gupta, Dericks P. Shukla, and A. P. Dimri. "Integrated approach for effective debris mapping in glacierized regions of Chandra River Basin, Western Himalayas, India." Science of The Total Environment 779 (July 2021): 146492. http://dx.doi.org/10.1016/j.scitotenv.2021.146492.

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Dissertations / Theses on the topic "Chandra basin"

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Talluri, Bharath Chandra [Verfasser]. "Mechanistic and neural basis of choice-induced biases in decision-making / Bharath Chandra Talluri." Hamburg : Staats- und Universitätsbibliothek Hamburg Carl von Ossietzky, 2020. http://d-nb.info/1232407801/34.

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Vernon, Rowan Emma. "Tectonic evolution and plateau uplift around the Changma Basin in the Qilian Mountains, NE Tibetan Plateau." Thesis, University of Leicester, 2016. http://hdl.handle.net/2381/37964.

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The Qilian Mountains are one of the most actively uplifting regions of the Tibetan Plateau and may provide a type example for the early evolution of its older regions. The mountains form a 300 km wide, NW – SE trending fold-thrust belt which extends 1000 km along the northeast margin of the Plateau and over-thrust the Hexi Corridor to the northeast and the Qaidam Basin to the southwest. An early-mid Palaeozoic orogenic suture belt, composed of faulted terranes of Late Proterozoic to early-mid Palaeozoic meta-sedimentary and meta-volcanic strata, is exposed in the Qilian Mountains and has been previously suggested to be reactivated by Late Cenozoic deformation. NE-directed crustal shortening, associated with the far-field effects of the Indo-Asian collision, has been active in the Qilian Mountains since the early-mid Miocene. It is characterised by the uplift of high mountain ranges along crustal scale thrust faults which splay south-eastwards from the sinistral-slip, north-northeast trending Altyn Tagh Fault and are postulated to connect along a shallow-dipping decollement in the midlower crust. Initiation of uplift in the Qilian Mountains was associated with a considerable decrease in the slip rate along the eastern end of the Altyn Tagh Fault and coincides with a plateau-wide reorganisation of deformation. This project presents new field mapping and remote sensing analysis and integrates this with existing geophysical data to i) understand and constrain the tectonic evolution of the northeast corner of the Qilian Mountains and the northwest corner of the Hexi Corridor, ii) examine the structural and lithological control of the Palaeozoic accretionary crust over Late Cenozoic deformation within the mountain ranges, and iii) establish the spatial and temporal extent of different styles of deformation within the northeastern Qilian Mountains.
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Books on the topic "Chandra basin"

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Orantin, Nicolas. Unitary integrals and related matrix models. Edited by Gernot Akemann, Jinho Baik, and Philippe Di Francesco. Oxford University Press, 2018. http://dx.doi.org/10.1093/oxfordhb/9780198744191.013.17.

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This article examines the basic properties of unitary matrix integrals using three matrix models: the ordinary unitary model, the Brézin-Gross-Witten (BGW) model and the Harish-Chandra-Itzykson-Zuber (HCIZ) model. The tricky sides of the story are given special attention, such as the de Wit-’t Hooft anomaly in unitary integrals and the problem of correlators with Itzykson-Zuber measure. The method of character expansions is also emphasized as a technical tool. The article first provides an overview of the theory of the BGW model, taking into account the de Wit-’t Hooft anomaly and the M-theory of matrix models, before discussing the theory of the HCIZ integral. In particular, it describes the basics of character calculus, character expansion of the HCIZ integral, character expansion for the BGW model and Leutwyler-Smilga integral, and pair correlator in HCIZ theory.
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Book chapters on the topic "Chandra basin"

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Singh, Rupendra, Rajesh Kumar, Syed Umer Latief, Rajesh Kumar, and Mayank Shekhar. "Recession of Gaglu Glacier, Chandra Basin, Western Indian Himalaya." In Springer Climate, 103–23. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-92782-0_5.

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Sahu, Rakesh, and R. D. Gupta. "Snow Cover Analysis in Chandra Basin of Western Himalaya from 2001 to 2016." In Lecture Notes in Civil Engineering, 557–66. Singapore: Springer Singapore, 2019. http://dx.doi.org/10.1007/978-981-13-7067-0_45.

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Sriram, S., and M. Geetha Priya. "The Contemporary State of Glacial Lakes in Chandra Basin, Western Himalayas: A Case Study in 2020." In Futuristic Communication and Network Technologies, 519–26. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-8338-2_43.

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Ramsankaran, RAAJ, Ankur Pandit, and Avinash Parla. "Decadal Estimates of Surface Mass Balance for Glaciers in Chandra Basin, Western Himalayas, India—A Geodetic Approach." In Climate Change Signals and Response, 109–25. Singapore: Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-13-0280-0_7.

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Geetha Priya, M., Ishmohan Bahuguna, D. Krishnaveni, and Suresh Devaraj. "Estimation of Geodetic Mass Balance for Bada Shigri Glacier and Samudra Tapu Glacier in Chandra Basin, India." In Water, Cryosphere, and Climate Change in the Himalayas, 101–13. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-67932-3_6.

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Sharma, Parmanand, Lavkush Kumar Patel, Ajit T. Singh, Thamban Meloth, and Rasik Ravindra. "Glacier Response to Climate in Arctic and Himalaya During Last Seventeen Years: A Case Study of Svalbard, Arctic and Chandra Basin, Himalaya." In Climate Change and the White World, 139–56. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-21679-5_10.

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KUMAR, PULLIGILLA MANOJ. "A contemplate on issues faced by scholars with English language while composing a research paper." In WRITING SKILLS FOR ACADEMIC RESEARCH, 218–33. Royal Book Publisher, 2021. http://dx.doi.org/10.26524/royal.55.13.

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Rao, V. Chandra. (2018). English is worldwide scholastic language. For the most part researchers are expected to distribute a paper globally. A scholastic composing style assumes a significant part in English to give certainty and effectives on their own point of view. English has extraordinary arrangements of rules significantly focus on jargon, accentuation, spellings, language, word sentences assumes key part for great scholarly composition. Utilize basic present or past tense just, dodge sentence length and excess.
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Stevens, John A. "Tensions and Transitions: 1870–77." In Keshab, 115–53. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190901752.003.0005.

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This chapter begins by discussing Keshab Chandra Sen’s attempts to replicate British models of liberal social reform in India. It goes on to examine Keshab’s changing attitudes to gender, reform and civilization, as he gradually moved away from the liberalism he had espoused in Britain. It argues that Ramakrishna exerted a considerable influence on Keshab, as he began to embrace aspects of Hindu revivalism and Indian nationalism. It argues that Keshab attempted to undermine the epistemological basis of British imperialism by arguing for the value of ‘madness’ and ‘inspiration’ as modes of thought.
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Chirikba, Viacheslav. "From the History of Abkhaz Romanized Alphabets." In Armenia, Caucaso e Asia Centrale Ricerche 2022. Venice: Fondazione Università Ca’ Foscari, 2023. http://dx.doi.org/10.30687/978-88-6969-667-1/001.

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The article discusses the vicissitudes around the adoption of two versions of the Abkhaz alphabet based on the Latin script – the ‘analytical’ alphabet, proposed by Academician Nikolai Marr (adopted in 1926 and used until 1928), and the ‘unified alphabet’, which replaced Marr’s alphabet. Marr’s system was, in fact, nothing more than a phonetic transcription, complex and inconvenient even for linguists, and unfit for school and literary purposes, which motivated the Abkhaz authorities to opt for its radical reform. The new Romanized alphabet was introduced into school practice in 1929 and functioned until 1938. There is some controversy as to the authorship of this script. In later literature it was attributed to N. Yakovlev, but in reality those who were directly involved in the creation of the new alphabetical system were Y. Polivanov, S. Chanba and M. Khashba, though the latter two did consult with Yakovlev. The fact that both Polivanov and Chanba were executed during Stalinist purges may explain the silencing of their names. By the mid-1930s, the Soviet government had started replacing Latin scripts with Cyrillic-based ones, but with two notable exceptions: in 1938, the alphabets of the Abkhazians and South Ossetians were transferred into a Georgian graphic basis. It was only in 1954, after the death of Stalin, that the Abkhazians returned to their erstwhile Cyrillic alphabet.
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Byun, Hi-Ryong, and Suk-Young Hong. "Monitoring Agricultural Drought in South Korea." In Monitoring and Predicting Agricultural Drought. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780195162349.003.0041.

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South Korea (hereinafter referred to as Korea) lies in the middle latitudes of the Northern Hemisphere. Until the 1960s, Korea was a typical agrarian country, with agriculture generating roughly half of its gross national product (GNP) and employing more than half of the labor force. Agriculture still plays an important role in the Korean national economy, but it accounts for a relatively much lower share of the GNP (5.3% in 1997) and engages much less of the population (11.0%). The agricultural share of the national economy is declining continuously. Farms in Korea, as in many other Asian countries, have traditionally been small. Average farm size has been growing slowly from 0.86 ha in 1960 to 1.39 ha in 2001, despite a significant reduction in the average number of persons per household engaged in farming—from 6.20 persons to 2.91 persons. As a result, agriculture has become more intensive. The country has four distinct seasons: summer, fall, winter, and spring. Summer and winter have a longer duration than spring or fall. The summer rainy season (Changma) in the Korean Peninsula includes the period from late June to late July. About three quarters of the annual precipitation falls during the summer season. The average annual precipitation in Korea is 1,274 mm, which is about 1.3 times the world average (973 mm). The variation in annual precipitation is larger, with an annual minimum of 784 mm and an annual maximum of 2675 mm in Seoul. Heavy rains fall during the Changma season, which is influenced by monsoons. The National Institute of Agricultural Science and Technology (NIAST) classified Korea (except Jeju Island) into 19 climate zones to efficiently use agricultural resources for wetland rice production. Among the 19 zones, zone 14, which is the Southern Charyeong Plain, yields the best harvest and the most stable rice production. Zones 11 (Yeongnam Basin), 17 (the northeastern coast), and 18 (the mid-eastern coast) are categorized as drought-risk areas at transplanting stage based on the ratio of evaporation to precipitation (Choi and Yun, 1989).
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Conference papers on the topic "Chandra basin"

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Nela, Bala Raju, Gulab Singh, and Anil V. Kulkarni. "Glacier Movement Estimation of Benchmark Glaciers in Chandra Basin Using Differential SAR Interferometry (DInSAR) Technique." In IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2019. http://dx.doi.org/10.1109/igarss.2019.8900537.

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Meshram, Kamini, Runa Antony, Laluraj C. M., Parmanand Sharma, and Ruben Sommaruga. "Nutrient (C, N, P) export from debris-covered and debris-free glaciers, Chandra basin, Western Himalaya." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.11904.

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Yunus, Muchammad, and Agus Wijaya. "Histopathological changes in gills of wild snakehead, Channa striata infected Trichodina sp. from Surabaya River." In THE 8TH INTERNATIONAL CONFERENCE AND WORKSHOP ON BASIC AND APPLIED SCIENCE (ICOWOBAS) 2021. AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0103705.

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Simmons, Kathy, and Budi Chandra. "Experimental Investigation Into the Performance of Shallow Aeroengine Off-Takes." In ASME Turbo Expo 2014: Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/gt2014-26132.

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Oil removal (scavenge) from aeroengine bearing chambers is an ongoing challenge for aeroengine designers. Effective scavenging of oil is necessary to avoid excessive heat generation, degradation of oil properties and deterioration in heat transfer functionality. However the task of oil removal is not trivial. Oil is entrained in a highly rotating environment induced by the rotating shafts. Simply removing a larger volume of fluid from the chamber with the scavenge pump can create higher air flowrates but lead to oil becoming trapped in the chamber and so no reduction in residence volume (the amount of oil present in the chamber during operation). The University of Nottingham Technology Centre in Gas Turbine Transmissions Systems has been conducting experiments investigating two phase behaviour within a simplified aeroengine bearing chamber operating at ambient pressures with water as the working liquid. The rig is constructed from polycarbonate enabling good visual access. In the chamber offtake region a number of behaviours can be observed relating to the hydraulic uplift and general flow behaviour as gas and liquid exit the chamber. Chandra et al [1] reports a parametric study using a design of experiments approach into geometrical variants of a shallow offtake region defined by curved approaches and a small offtake volume. Phenomenlogical factors were quantified and used to identify the best performing geometry. Previous work at the UTC [2, 3] has used residence volume as the primary comparative performance parameter. In this paper residence volume data is obtained for two sumps for which phenomenological data exists. The paper compares performance on the basis of these visual factors with performance on the basis of residence volume and concludes that although both frameworks have value, they do not lead to identical conclusions for all operating conditions. In film dominated cases significant hydraulic uplift usually corresponds to larger residence volume but for droplet dominated cases this is not necessarily so.
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